Influence of Terrain Factors on Soil Organic Carbon Stock in Pinus kesiya var. langbianensis Plantation

JIA Chen-xin-zhuo; LI Shuai-feng; SU Jian-rong

Volume 29 Issue 3

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Influence of Terrain Factors on Soil Organic Carbon Stock in Pinus kesiya var. langbianensis Plantation

1.
Research Institute of Resource Insects, Chinese Academy of Forestry, Kunming 650224, Yunnan, China
2.
Pu'er Forest Ecosystem Research Station, State Forestry Administration, Kunming 650224, Yunnan, China

Received Date: 2015-12-25

Abstract

[Objective] Taking middle-aged Pinus kesiya var. langbianensis plantations as examples to study the influence of terrain factors on soil organic carbon (SOC) reserve in P. kesiya var. langbianensis plantations.[Method] The differences in SOC contents, total nitrogen, soil bulk density, C:N ratio and SOC reserve among different soil layers under different site conditions were analyzed using T test and single factor analysis of variance, and the Pearson correlation between SOC reserve and total nitrogen, bulk density, C:N ratio was evaluated.[Result] The results showed that the SOC content, total nitrogen and C:N ratio decreased with the soil depth, while the bulk density increased. The aspect and slope had a significant effect on SOC reserve. The effect was significantly higher in shady slope than in sunny slope and significantly lower in slope 20~30° than in slopes 10~20° and 0~10°. But the slope position has no significant effect on SOC reserve. For 0~100 cm soil layer, the SOC reserve showed a tendency of reduction with the soil depth at different site conditions of middle-aged P. kesiya var. langbianensis plantation. And the SOC reserve was significantly higher among 0-20 cm soil layer at different aspect, slope position and slope degree. But the aspect and slope degree had a significant impact on the SOC reserve of 0-20 cm (P[Conclusion] The results suggested that the site conditions would influence the size and distribution of carbon storage, especially the aspect and slope would cause the difference of SOC storage in middle-aged P. kesiya var. langbianensis plantation.
- Pinus kesiya var. langbianensis,
- plantation,
- middle-aged forest,
- SOC stocks

References

[1]	Vesterdal L, Clarke N, Sigurdsson B D, et al. Do tree species influence soil carbon stocks in temperate and boreal forests?[J]. Forest Ecology and Management, 2013, (309):4-18.
[2]	Batlle-Bayer L, Batjes N H, Bindraban P S. Changes in organic carbon stocks upon land use conversion in the Brazilian Cerrado:a review[J]. Agriculture, Ecosystems & Environment, 2010, 137(1):47-58.
[3]	Groffmann P M, Zak D R, Christensen S, et al. Early spring nitrogen dynamics in a temperate forest landscape[J]. Ecology, 1993, 74(5):1579-1585.
[4]	Hansson K, Helmisaari H S, Sah S P, et al. Fine root production and turnover of tree and understorey vegetation in Scots pine, silver birch and Norway spruce stands in SW Sweden[J]. Forest Ecology and Management, 2013, (309):58-65.
[5]	Davidson E A, Trumbore S E, Amundson R. Biogeochemistry:soil warming and organic carbon content[J]. Nature, 2000, 408(6814):789-790.
[6]	Lamparter A, Bachmann J, Goebel M O, et al. Carbon mineralization in soil:Impact of wetting-drying, aggregation and water repellency[J]. Geoderma, 2009, 150(3):324-333.
[7]	Hao Y, Lal R, Owens L B, et al. Effect of cropland management and slope position on soil organic carbon pool at the North Appalachian Experimental Watersheds[J]. Soil and Tillage Research, 2002, 68(2):133-142.
[8]	谢锦升. 植被恢复对退化红壤易变碳及土壤呼吸的影响[D]. 北京:北京林业大学, 2005.
[9]	Miller A E, Schimel J P, Meixner T, et al. Episodic rewetting enhances carbon and nitrogen release from chaparral soils[J]. Soil Biology and Biochemistry, 2005, 37(12):2195-2204.
[10]	方华军, 杨学明, 张晓平, 等. 坡耕地黑土活性有机碳空间分布及生物有效性[J]. 水土保持学报, 2006, 20(2):59-63.
[11]	李帅锋,苏建荣,刘万德,等,2013云南省思茅松林群落数量分类及物种多样性与自然环境的关系[J]. 生态学杂志, 2013, 32(12):3152-3159.
[12]	Li S, Su J, Liu W, et al. Changes in Biomass Carbon and Soil Organic Carbon Stocks following the Conversion from a Secondary Coniferous Forest to a Pine Plantation[J]. PloS One, 2015, 10(9):e0135946.
[13]	陈伟, 孟梦, 李江, 等. 思茅松人工林土壤有机碳库特征[J]. 中国水土保持科学, 2014, 12(2):105-112.
[14]	李帅锋,苏建荣,刘万德, 等. 思茅松人工林土壤有机碳和氮储量变化[J]. 林业科学研究,2015, 28(6):810-817.
[15]	刘小菊, 苏静霞, 石亮.思茅松人工林生长与立地条件的关系研究[J].中国农学通报, 2010, 26(18):142-145.
[16]	Ellert B H, Bettany J R. Calculation of organic matter and nutrients stored in soils under contrasting management regimes[J]. Canadian Journal of Soil Science, 1995, 75(4):529-538.
[17]	Wellock M L, LaPerle C M, Kiely G. What is the impact of afforestation on the carbon stocks of Irish mineral soils?[J]. Forest Ecology and Management, 2011, 262(8):1589-1596.
[18]	刘世荣, 王晖, 栾军伟. 中国森林土壤碳储量与土壤碳过程研究进展[J]. 生态学报, 2011, 31(19):5437-5448.
[19]	于振良. 我国主要森林生态系统碳贮量和碳平衡[J]. 植物生态学报, 2000, 24(5):518-522.
[20]	黄从德, 张健, 杨万勤, 等. 四川森林土壤有机碳储量的空间分布特征[J]. 生态学报, 2009, 29(3):1217-1225.
[21]	孟梦, 李江, 李莲芳, 等. 思茅松人工林凋落物量及其分解状况研究[J]. 西部林业科学, 2011, 40(2):56-63.
[22]	徐侠, 陈月琴, 汪家社, 等. 武夷山不同海拔高度土壤活性有机碳变化[J]. 应用生态学报, 2008, 19(3):539-544.
[23]	Mueller K E, Eissenstat D M, Hobbie S E, et al. Tree species effects on coupled cycles of carbon, nitrogen, and acidity in mineral soils at a common garden experiment[J]. Biogeochemistry, 2012, 111(1-3):601-614.
[24]	Santantonio D, Hermann R K, Overton W S. Root biomass studies in forest ecosystems[J]. Pedobiologia, 1977, 17:1-31.
[25]	Poeplau C, Don A, Vesterdal L, et al. Temporal dynamics of soil organic carbon after land-use change in the temperate zone-carbon response functions as a model approach[J]. Global Change Biology, 2011, 17(7):2415-2427.
[26]	宋娅丽, 康峰峰, 韩海荣, 等. 自然因子对中国森林土壤碳储量的影响分析[J]. 世界林业研究, 2015, 28(3):6-12.
[27]	White R E, Haigh R A, Macduff J H. Frequency distributions and spatially dependent variability of ammonium and nitrate concentrations in soil under grazed and ungrazedgrassland[J]. Fertilizer Research, 1987, 11(3):193-208.
[28]	Jiang Y J, Yuan D X, Zhang C, et al. Impact of land-use change on soil properties in a typical karst agricultural region of Southwest China:a case study of Xiaojiang watershed, Yunnan[J]. Environmental Geology, 2006, 50(6):911-918.

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通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

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Influence of Terrain Factors on Soil Organic Carbon Stock in Pinus kesiya var. langbianensis Plantation

1. Research Institute of Resource Insects, Chinese Academy of Forestry, Kunming 650224, Yunnan, China

2. Pu'er Forest Ecosystem Research Station, State Forestry Administration, Kunming 650224, Yunnan, China

Received Date: 2015-12-25

Abstract: [Objective] Taking middle-aged Pinus kesiya var. langbianensis plantations as examples to study the influence of terrain factors on soil organic carbon (SOC) reserve in P. kesiya var. langbianensis plantations.[Method] The differences in SOC contents, total nitrogen, soil bulk density, C:N ratio and SOC reserve among different soil layers under different site conditions were analyzed using T test and single factor analysis of variance, and the Pearson correlation between SOC reserve and total nitrogen, bulk density, C:N ratio was evaluated.[Result] The results showed that the SOC content, total nitrogen and C:N ratio decreased with the soil depth, while the bulk density increased. The aspect and slope had a significant effect on SOC reserve. The effect was significantly higher in shady slope than in sunny slope and significantly lower in slope 20~30° than in slopes 10~20° and 0~10°. But the slope position has no significant effect on SOC reserve. For 0~100 cm soil layer, the SOC reserve showed a tendency of reduction with the soil depth at different site conditions of middle-aged P. kesiya var. langbianensis plantation. And the SOC reserve was significantly higher among 0-20 cm soil layer at different aspect, slope position and slope degree. But the aspect and slope degree had a significant impact on the SOC reserve of 0-20 cm (P[Conclusion] The results suggested that the site conditions would influence the size and distribution of carbon storage, especially the aspect and slope would cause the difference of SOC storage in middle-aged P. kesiya var. langbianensis plantation.

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[1]	Vesterdal L, Clarke N, Sigurdsson B D, et al. Do tree species influence soil carbon stocks in temperate and boreal forests?[J]. Forest Ecology and Management, 2013, (309):4-18.
[2]	Batlle-Bayer L, Batjes N H, Bindraban P S. Changes in organic carbon stocks upon land use conversion in the Brazilian Cerrado:a review[J]. Agriculture, Ecosystems & Environment, 2010, 137(1):47-58.
[3]	Groffmann P M, Zak D R, Christensen S, et al. Early spring nitrogen dynamics in a temperate forest landscape[J]. Ecology, 1993, 74(5):1579-1585.
[4]	Hansson K, Helmisaari H S, Sah S P, et al. Fine root production and turnover of tree and understorey vegetation in Scots pine, silver birch and Norway spruce stands in SW Sweden[J]. Forest Ecology and Management, 2013, (309):58-65.
[5]	Davidson E A, Trumbore S E, Amundson R. Biogeochemistry:soil warming and organic carbon content[J]. Nature, 2000, 408(6814):789-790.
[6]	Lamparter A, Bachmann J, Goebel M O, et al. Carbon mineralization in soil:Impact of wetting-drying, aggregation and water repellency[J]. Geoderma, 2009, 150(3):324-333.
[7]	Hao Y, Lal R, Owens L B, et al. Effect of cropland management and slope position on soil organic carbon pool at the North Appalachian Experimental Watersheds[J]. Soil and Tillage Research, 2002, 68(2):133-142.
[8]	谢锦升. 植被恢复对退化红壤易变碳及土壤呼吸的影响[D]. 北京:北京林业大学, 2005.
[9]	Miller A E, Schimel J P, Meixner T, et al. Episodic rewetting enhances carbon and nitrogen release from chaparral soils[J]. Soil Biology and Biochemistry, 2005, 37(12):2195-2204.
[10]	方华军, 杨学明, 张晓平, 等. 坡耕地黑土活性有机碳空间分布及生物有效性[J]. 水土保持学报, 2006, 20(2):59-63.
[11]	李帅锋,苏建荣,刘万德,等,2013云南省思茅松林群落数量分类及物种多样性与自然环境的关系[J]. 生态学杂志, 2013, 32(12):3152-3159.
[12]	Li S, Su J, Liu W, et al. Changes in Biomass Carbon and Soil Organic Carbon Stocks following the Conversion from a Secondary Coniferous Forest to a Pine Plantation[J]. PloS One, 2015, 10(9):e0135946.
[13]	陈伟, 孟梦, 李江, 等. 思茅松人工林土壤有机碳库特征[J]. 中国水土保持科学, 2014, 12(2):105-112.
[14]	李帅锋,苏建荣,刘万德, 等. 思茅松人工林土壤有机碳和氮储量变化[J]. 林业科学研究,2015, 28(6):810-817.
[15]	刘小菊, 苏静霞, 石亮.思茅松人工林生长与立地条件的关系研究[J].中国农学通报, 2010, 26(18):142-145.
[16]	Ellert B H, Bettany J R. Calculation of organic matter and nutrients stored in soils under contrasting management regimes[J]. Canadian Journal of Soil Science, 1995, 75(4):529-538.
[17]	Wellock M L, LaPerle C M, Kiely G. What is the impact of afforestation on the carbon stocks of Irish mineral soils?[J]. Forest Ecology and Management, 2011, 262(8):1589-1596.
[18]	刘世荣, 王晖, 栾军伟. 中国森林土壤碳储量与土壤碳过程研究进展[J]. 生态学报, 2011, 31(19):5437-5448.
[19]	于振良. 我国主要森林生态系统碳贮量和碳平衡[J]. 植物生态学报, 2000, 24(5):518-522.
[20]	黄从德, 张健, 杨万勤, 等. 四川森林土壤有机碳储量的空间分布特征[J]. 生态学报, 2009, 29(3):1217-1225.
[21]	孟梦, 李江, 李莲芳, 等. 思茅松人工林凋落物量及其分解状况研究[J]. 西部林业科学, 2011, 40(2):56-63.
[22]	徐侠, 陈月琴, 汪家社, 等. 武夷山不同海拔高度土壤活性有机碳变化[J]. 应用生态学报, 2008, 19(3):539-544.
[23]	Mueller K E, Eissenstat D M, Hobbie S E, et al. Tree species effects on coupled cycles of carbon, nitrogen, and acidity in mineral soils at a common garden experiment[J]. Biogeochemistry, 2012, 111(1-3):601-614.
[24]	Santantonio D, Hermann R K, Overton W S. Root biomass studies in forest ecosystems[J]. Pedobiologia, 1977, 17:1-31.
[25]	Poeplau C, Don A, Vesterdal L, et al. Temporal dynamics of soil organic carbon after land-use change in the temperate zone-carbon response functions as a model approach[J]. Global Change Biology, 2011, 17(7):2415-2427.
[26]	宋娅丽, 康峰峰, 韩海荣, 等. 自然因子对中国森林土壤碳储量的影响分析[J]. 世界林业研究, 2015, 28(3):6-12.
[27]	White R E, Haigh R A, Macduff J H. Frequency distributions and spatially dependent variability of ammonium and nitrate concentrations in soil under grazed and ungrazedgrassland[J]. Fertilizer Research, 1987, 11(3):193-208.
[28]	Jiang Y J, Yuan D X, Zhang C, et al. Impact of land-use change on soil properties in a typical karst agricultural region of Southwest China:a case study of Xiaojiang watershed, Yunnan[J]. Environmental Geology, 2006, 50(6):911-918.

Influence of Terrain Factors on Soil Organic Carbon Stock in Pinus kesiya var. langbianensis Plantation

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通讯作者: 陈斌, bchen63@163.com

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Influence of Terrain Factors on Soil Organic Carbon Stock in Pinus kesiya var. langbianensis Plantation

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